[10] Roubinet , Moreira, Noble Gas Systematics in MORBs and OIBs and Reconstitution of the Time-Evolution of Mantle Composition for Heavy Noble Gases: the Role of Subduction of Atmospheric Noble Gases. AGU 2014

[13] Chaussidon M. and Bischoff A., Is there a difference in age of formation and precursor composition between large and normal chondrules? 77th annual meeting of the Meteoritical Society, abstract #5256.
[14] Chaussidon M., Oxygen and Magnesium isotopic constraints on the presence of planetary fragments in meteoritic chondrules, ACCRETE meeting, Nice, 2014

[15] Charnoz. Evolution of the protolunar disk and constrains on the origin of the Moon. Invited talk. PURE workshop (IPGP, 2014)

[17] Roubinet , Moreira, Noble Gas Systematics in MORBs and OIBs and Reconstitution of the Time-Evolution of Mantle Composition for Heavy Noble Gases: the Role of Subduction of Atmospheric Noble Gases. AGU 2014

[2] C. Michaut and C. Thorey (présentation invitée), Consequences of the low density of the primary crust on the magmatic history of the Moon, Abstract P51H-05 presented at Fall Meeting, AGU, San Francisco, CA, 9-13 Dec, 2013.

Seven of our permanent members are professor or assistant professor, so they do their regular teaching duty and several lectures are directly connected to the labex activity (planet formation, cosmochemistry, interior and structure of Earths etc;.)